Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/85935
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dc.contributor.authorMarchant, T.R.-
dc.contributor.authorRoberts, A.J.-
dc.date.issued1987-
dc.identifier.citationAustralia and New Zealand Industrial and Applied Mathematics (ANZIAM) Journal, 1987; 29(1):103-125-
dc.identifier.issn0334-2700-
dc.identifier.issn1839-4078-
dc.identifier.urihttp://hdl.handle.net/2440/85935-
dc.description.abstractShort-crested waves are defined as propagating surface gravity waves which are doubly-periodic in the horizontal plane. Linearly, the short-crested wave system we consider occurs when two progressive wavetrains of equal amplitude and frequency are propagating at an angle to each other. Solutions are calculated via a computer-generated perturbation expansion in wave steepness. Harmonic resonance affects the solutions but Padé approximants can be used to estimate wave properties such as maximum wave steepness, frequency, kinetic energy and potential energy. The force exerted by waves being reflected by a seawall is also calculated. Our results for the maximum depth-integrated onshore wave force in the standing wave limit are compared with experiment. The maximum force exerted on a seawail occurs for a steep wave in shallow water incident at an oblique angle. Results are given for this maximum force.-
dc.description.statementofresponsibilityT. R. Marchant and A. J. Roberts-
dc.language.isoen-
dc.publisherAustralian Mathematical Society-
dc.rights© Copyright Australian Mathematical Society 1987-
dc.source.urihttp://dx.doi.org/10.1017/s0334270000005658-
dc.titleProperties of short-crested waves in water of finite depth-
dc.typeJournal article-
dc.identifier.doi10.1017/S0334270000005658-
pubs.publication-statusPublished-
dc.identifier.orcidRoberts, A.J. [0000-0001-8930-1552]-
Appears in Collections:Aurora harvest 2
Mathematical Sciences publications

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